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                <text>&lt;h2&gt;Alkali feldspar&lt;/h2&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;(K,Na)[AlSi&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;8&lt;/sub&gt;]&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Framework silicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;monoclinic (-) or triclinic (+) (-)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;&lt;span&gt;Colour in hand specimen:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; white or pink&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Cleavage:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; two at 90°&lt;/span&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;&lt;span&gt;Hardness:&lt;/span&gt;&lt;/em&gt;&lt;span&gt; 6-6.5&lt;/span&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;colourless&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;none&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Relief:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;low&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Birefringence:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;~0.008; 1&lt;sup&gt;st&lt;/sup&gt;&lt;span&gt; &lt;/span&gt;order greys&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Extinction:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;inclined&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;em&gt;Twinning: &lt;/em&gt;usually simple or lamellar;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;              Microcline (KAlSi&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;8&lt;/sub&gt;) displays characteristic cross-hatched twinning&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p class="NoSpacing"&gt;&lt;strong&gt;&lt;span&gt;M400 &lt;/span&gt;&lt;/strong&gt;&lt;strong&gt;&lt;span&gt;Alkali feldspar, microcline&lt;/span&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;A single crystal of pale orange-pink alkali feldspar.&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Pearly lustre.&lt;/p&gt;
&lt;p class="NoSpacing"&gt;&lt;strong&gt;&lt;span&gt;M401 &lt;/span&gt;&lt;/strong&gt;&lt;strong&gt;&lt;span&gt;Alkali feldspar, orthoclase&lt;/span&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;strong&gt;Norway&lt;/strong&gt;&lt;strong&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;A fragment of opaque, pale grey alkali feldspar.&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Two sets of good cleavage at right angles, with a pearly lustre on the cleavage faces.&lt;/p&gt;
&lt;p class="NoSpacing"&gt;&lt;strong&gt;&lt;span&gt;M402 &lt;/span&gt;&lt;/strong&gt;&lt;strong&gt;&lt;span&gt;Alkali feldspar, orthoclase&lt;/span&gt;&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;&lt;strong&gt;Shap, Westmorland&lt;/strong&gt;&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Porphyritic granite.&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Large phenocrysts of pink feldspar, two sets of cleavage at 90°, simple twinning.&lt;span&gt; &lt;/span&gt;&lt;br class="NoSpacing" /&gt;Also white plagioclase feldspar, quartz and biotite&lt;strong&gt;.&lt;/strong&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l100"&gt;L100 Alkali granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l101"&gt;L101 Granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l102"&gt;L102 Hornblende biotite granite&lt;/a&gt;&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l110"&gt;L110 Rhyolite, porphyritic (quartz porphyry)&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;alkali feldspar&lt;/div&gt;
&lt;/div&gt;
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            <name>Title</name>
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                <text>&lt;h2&gt;Tourmaline&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>&lt;span&gt;Tourmaline is the only common mineral of which boron is an essential constituent. Its presence in a rock, therefore, indicates that the rock contains significant boron. &lt;/span&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;div class="element-text"&gt;(Na,Ca)(Mg,Fe,Mn,Li,Al)&lt;sub&gt;3&lt;/sub&gt;(Al,Mg,Fe&lt;sup&gt;3+&lt;/sup&gt;)&lt;sub&gt;6&lt;/sub&gt;[Si&lt;sub&gt;6&lt;/sub&gt;O&lt;sub&gt;18&lt;/sub&gt;](BO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;(O,OH)&lt;sub&gt;3&lt;/sub&gt;(OH,F)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Ring silicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;trigonal (-)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in hand specimen:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;black&lt;br /&gt;&lt;em&gt;Hardness:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;7&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;typically brown-green or green&lt;br /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;strongly pleochroic in many colours&lt;br /&gt;&lt;em&gt;Relief:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;moderate&lt;br /&gt;&lt;em&gt;Birefringence:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;typically 2nd order&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/metamorphic-rocks/l504"&gt;L504 Garnet schist&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;tourmaline&lt;/div&gt;
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        <name>pegmatite</name>
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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;Zircon&lt;/h2&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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              <elementText elementTextId="136">
                <text>&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h3&gt;Formula&lt;/h3&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;Zr[SiO&lt;sub&gt;4&lt;/sub&gt;]&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Structure&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Orthosilicate&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Crystal System&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Crystal system:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;tetragonal (+)&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Physical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in hand specimen:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;reddish brown, yellow, grey, green or colourless&lt;br /&gt;&lt;em&gt;Hardness:&lt;/em&gt;&lt;span&gt; &lt;/span&gt;7.5&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Optical Properties&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Colour in plane polarised light:&lt;/em&gt; colourless to pale brown&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;em&gt;Pleochroism:&lt;/em&gt; very weak&lt;br /&gt;&lt;em&gt;Relief:&lt;/em&gt; high&lt;br /&gt;&lt;em&gt;Birefringence:&lt;/em&gt; 0.042-0.065; 3rd order green to 4th order green&lt;br /&gt;&lt;em&gt;Extinction:&lt;/em&gt; straight&lt;br /&gt;&lt;em&gt;Twinning:&lt;/em&gt; rare&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Rock Specimens&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/igneous-rocks/l100"&gt;L100 Alkali granite&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Mineral Name&lt;/h3&gt;
&lt;div class="element-text"&gt;zircon&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>Zircon is a common accessory mineral of many igneous rocks. Pleochroic haloes are formed by damage to the crystal lattice of enclosing minerals by the radioactive decay of elements such as Th and U in zircon. These may be particularly noticeable in biotite grains in old granitic rocks.</text>
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        <name>thorium</name>
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                <text>&lt;h2&gt;&lt;strong&gt;L102&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Hornblende biotite granite&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Caledonian, Devonian&lt;/p&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Glencoe&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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&lt;h3&gt;&lt;span style="font-size:14px;"&gt;Hand Specimen&lt;/span&gt;&lt;/h3&gt;
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&lt;p&gt;Medium to coarse-grained rock with a&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/203"&gt;granular&lt;/a&gt;&lt;span&gt; &lt;/span&gt;texture.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;White feldspar&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/215"&gt;laths&lt;/a&gt;&lt;span&gt; &lt;/span&gt;2-4 mm long are clearly visible.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Other phases: pink feldspar, black biotite mica, black hornblende amphibole and pale grey quartz. These grains are more&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/188"&gt;equant&lt;/a&gt;, typically 1-2 mm across.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;Biotite may be distinguished from hornblende by its flaky&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/206"&gt;habit&lt;/a&gt;&lt;span&gt; &lt;/span&gt;and one good&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/180"&gt;cleavage&lt;/a&gt;. It is shinier than hornblende.&lt;/p&gt;
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&lt;h3&gt;Thin-section&lt;/h3&gt;
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&lt;p&gt;Plagioclase feldspar&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- The larger laths (2-4 mm long) are strongly&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/267"&gt;zoned&lt;/a&gt;. The cores of these laths, which display clear&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/169"&gt;lamellar twinning&lt;/a&gt;, have been&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/232"&gt;overgrown&lt;/a&gt;&lt;span&gt; &lt;/span&gt;by rims of more feldspar. Some&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/170"&gt;alteration&lt;/a&gt;&lt;span&gt; &lt;/span&gt;to white mica.&lt;/p&gt;
&lt;p&gt;Biotite mica&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- Grains typically 1 mm across. Strongly pleochroic in reddish brown and pale straw. Often associated with small grains of an opaque accessory mineral, probably magnetite.&lt;/p&gt;
Quartz&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- Grains are 1-2 mm across,&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/173"&gt;anhedral&lt;/a&gt;, and display&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/263"&gt;undulose extinction&lt;/a&gt;.
&lt;p&gt;Alkali feldspar&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- Anhedral grains up to 5mm long. Some alteration to white mica. Some grains display a&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/228"&gt;microperthite texture&lt;/a&gt;.&lt;/p&gt;
&lt;p&gt;Hornblende amphibole&lt;span&gt; &lt;/span&gt;&lt;br /&gt;- Pale green, anhedral. Grains appear to have been “eaten away”, reducing their&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/246"&gt;prismatic&lt;/a&gt;&lt;span&gt; &lt;/span&gt;form (diamond) to a ragged anhedral&lt;span&gt; &lt;/span&gt;&lt;a href="/p1acollections/items/show/206"&gt;form&lt;/a&gt;. Amphiboles have two cleavage planes which intersect at 56°.&lt;/p&gt;
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&lt;h3&gt;Rock History&lt;/h3&gt;
&lt;div class="element-text"&gt;This coarse-grained rock must have cooled slowly as part of an intrusion.&lt;br /&gt;&lt;br /&gt;Its granitic composition (essential quartz and feldspar) indicates that it was produced in a continental setting.&lt;br /&gt;&lt;br /&gt;Strongly zoned plagioclase crystals and “eaten away” appearance of the hornblende could be due to a change in the composition of the liquid from which the phases crystallised; perhaps due to magma mixing or degassing of volatiles from the magma.&lt;span&gt; &lt;/span&gt;&lt;br /&gt;&lt;br /&gt;Presence of hornblende and biotite indicate that this is a wet granite, probably from a subduction zone.&lt;br /&gt;&lt;br /&gt;Hydrothermal alteration of feldspars to white mica.&lt;/div&gt;
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&lt;h3&gt;Advanced Notes&lt;/h3&gt;
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&lt;p&gt;This rock is classified as an&lt;span&gt; &lt;/span&gt;&lt;span&gt;adamellite&lt;/span&gt;&lt;span&gt; &lt;/span&gt;because it contains roughly equal proportions of alkali feldspar and plagioclase feldspar, with additional quartz and biotite.&lt;/p&gt;
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&lt;h3&gt;Rock Name&lt;/h3&gt;
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&lt;p&gt;hornblende biotite granite&lt;br /&gt;adamellite&lt;/p&gt;
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